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A summary of consistently dated Atlantic sediment cores over the last 40 thou...
Rapid changes in ocean circulation and climate have been observed in marine-sediment and ice cores over the last glacial period and deglaciation, highlighting the non-linear... -
Distribution of planktic foraminifera at the last glacial maximum
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Content of different diatom species in sediment core GIK23414-6 and -9
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Content of different diatom species in sediment core GIK23411-5
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(Table A1) Ostracoda abundances in sediment core GIK23414-9
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List of cores with links to documentation datasets
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Last Interglacial synthesis of high-latitude temperature: temperature anomali...
The Last Interglacial (LIG, 129-116 thousand of years BP, ka) represents a test bed for climate model feedbacks in warmer-than-present high latitude regions. However, mainly... -
Last Glacial Maximum seawater temperature estimates based on planktonic foram...
Estimates of Last Glacial Maximum annual mean seawater temperatures at 50 m depth. The temperature estimates are derived using the Modern Analogue Technique using the ForCenS... -
Compiled reservoir ages from sediment cores from the Northeast Atlantic
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Annual SST estimates from the late Marine Isotope Stage 6 (140-135 kyr) and c...
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Relative abundance of Amphimelissa setosa in core sediments and the interpola...
BEA: Beaufort Sea; BER: Bering Sea; CHU: Chukchi Sea; ECS: East China Sea; ESS: East Siberian Sea; GOA: Gulf of Alaska; GRE: Greenland Sea; ICE: Iceland Sea; NOR: Norwegian Sea;... -
Maximum annual SST estimates during the early LIG (129-124 ka; 189 sites)
Drift correction has not been applied to the two coral sites!Drift correction could not be applied to four sites in a land box when located using OFES. -
SST estimates for the Last Interglacial (129-116 ka BP) during the months of ...
Drift correction has not been applied to the two coral sites!Drift correction could not be applied to four sites in a land box when located using OFES. -
SST estimates for the Last Interglacial (129-116 ka BP) during the months of ...
Note, that we have assumed a thermal equator of 5 degrees North, where sites above this latitude 'Summer' = JJA, and 'Winter' = DJF. Sites south of this line have 'Summer'... -
Annual SST estimates for the Last Interglacial (129-116 ka BP)
Drift correction has not been applied to the two coral sites!Drift correction could not be applied to four sites in a land box when located using OFES. -
Metadata for a compilation of 127 benthic δ¹³C time series (20-6 ka)
Abbreviations for ocean and sea regionsINA: intermediate North Atlantic OceanUDNA: upper deep North Atlantic OceanLDNA: lower deep North Atlantic OceanISA: intermediate South... -
Sea surface temperature estimates from several sediment cores in the North At...
Here, we have calculated new sea-surface temperature estimates over Dansgaard-Oeschger (DO) events 5-8 (c. 30-40 ka) from 14 sites in the North Atlantic, based on previously... -
Correlations between the proxy SST anomalies (annual, boreal summer and borea...
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Sea surface temperature estimation (Uk37) of several sediment cores in the ea...
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Sedimentation rates of surface sediments, a compilation from different sources
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